Hydrous Melting
Hydrous Melting is a geochemical process in the context of partial melting whereby the presence of water or other volatile components reduces the melting temperature of silicate minerals, thereby facilitating magma generation at lower temperatures compared to dry melting conditions.
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2017–2026
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Centre National de la Recherche Scientifique
Paris, France
28 h-index
102 publications
4.8K citations
University of Bayreuth
Bayreuth, Germany
27 h-index
71 publications
7.7K citations

Leibniz University Hannover
Hanover, Germany
23 h-index
55 publications
5.8K citations

Carnegie Institution for Science
Washington, United States
19 h-index
30 publications
3.3K citations
The University of Tokyo
Tokyo, Japan
15 h-index
31 publications
2.5K citations

Chinese Academy of Sciences
Beijing, China
13 h-index
49 publications
2.5K citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
13 h-index
27 publications
2K citations
Massachusetts Institute of Technology
Cambridge, United States
12 h-index
25 publications
4.3K citations
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